Inception of anthropogenic activities and palaeoclimatic reconstruction during the Late Holocene from a high-altitude region, Western Himalaya, India: Palynological perspective

IF 4.7 2区 地球科学 Q2 ENVIRONMENTAL SCIENCES
Anthropocene Pub Date : 2026-03-01 Epub Date: 2026-01-06 DOI:10.1016/j.ancene.2026.100526
Amit Kumar Mishra , Ruchika Bajpai Mohanty , Ratan Kar
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引用次数: 0

Abstract

Palynological analyses of surface soil and sub-surface sediments were undertaken from Chopta-Tungnath, Uttarakhand State, India, to decipher the Late Holocene climatic changes, along with the inception, intensification and impact of anthropogenic activities in this high-altitude Himalayan region. The study area is characterised by mixed-temperate forests and alpine meadows. The development of modern palynological analogues has been done by the surface soil samples that were collected along an altitudinal transect (2700–3680 m), encompassing three distinct vegetation zones: mixed-temperate forests, tree-line vegetation, and alpine-scrub and meadows. The modern analogues were primarily generated to interpret the pollen-vegetation relationship and are compatible with the sub-surface fossil pollen records. Sub-surface sampling was done from a trial trench (105 cm), dug in the zone of mixed-temperate forests. Based on the radiocarbon dates (14C), climate fluctuations over the last 5070 years have been inferred through variations in the ratio of arboreal to non-arboreal pollen (AP/NAP), along with the subtle variations in the frequencies of temperate broad-leaved taxa. Besides, deducing the Late Holocene climatic changes, the palynological assemblages were also used to record the anthropogenic activities in the region. Around 850 yr BP, the evidence of human impact is manifested by the declining trend in the pollen frequencies of Quercus and Rhododendron, which indicate the degradation of these two arboreal components of the forest. There is a corresponding spike of Asteroideae, Cichorioideae and ruderal pollen, which are related to human activities. The increasing frequencies of coprophilous (dung-loving) fungi in the palynological assemblages of the sub-surface sediments, around 900 yr BP, provide further evidence towards the introduction of grazers in the area.
印度西喜马拉雅高海拔地区晚全新世人类活动开始与古气候重建:孢粉学视角
对印度北阿坎德邦(Uttarakhand) Chopta-Tungnath地区表层土壤和次表层沉积物进行孢粉学分析,以揭示该地区晚全新世的气候变化,以及人类活动的开始、加剧和影响。研究区域的特点是混合温带森林和高山草甸。现代孢粉学类似物的发展是通过沿海拔样带(2700-3680 m)收集的表层土壤样本完成的,包括三个不同的植被带:混合温带森林,树线植被,高山灌丛和草甸。现代类似物的产生主要是为了解释花粉与植被的关系,并与地下化石花粉记录相一致。地下采样是在混合温带森林区挖的一条试验沟(105 cm)进行的。基于放射性碳测年(14C),通过树木花粉与非树木花粉的比值(AP/NAP)的变化,以及温带阔叶分类群频率的细微变化,推断了过去5070年的气候波动。此外,孢粉组合还用于推断晚全新世的气候变化,记录了该地区的人类活动。在850 yr BP左右,人类影响的证据表现为栎科和杜鹃花的花粉频率呈下降趋势,这表明森林中这两种乔木成分的退化。与之相对应的菊科、菊科和菊科花粉均有穗状分布,与人类活动有关。大约900 年BP的次表层沉积物孢粉组合中粪菌(粪菌)的频率增加,为该地区引入食草动物提供了进一步的证据。
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来源期刊
Anthropocene
Anthropocene Earth and Planetary Sciences-Earth and Planetary Sciences (miscellaneous)
CiteScore
6.30
自引率
0.00%
发文量
27
审稿时长
102 days
期刊介绍: Anthropocene is an interdisciplinary journal that publishes peer-reviewed works addressing the nature, scale, and extent of interactions that people have with Earth processes and systems. The scope of the journal includes the significance of human activities in altering Earth’s landscapes, oceans, the atmosphere, cryosphere, and ecosystems over a range of time and space scales - from global phenomena over geologic eras to single isolated events - including the linkages, couplings, and feedbacks among physical, chemical, and biological components of Earth systems. The journal also addresses how such alterations can have profound effects on, and implications for, human society. As the scale and pace of human interactions with Earth systems have intensified in recent decades, understanding human-induced alterations in the past and present is critical to our ability to anticipate, mitigate, and adapt to changes in the future. The journal aims to provide a venue to focus research findings, discussions, and debates toward advancing predictive understanding of human interactions with Earth systems - one of the grand challenges of our time.
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